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Geochemistry Of Groundwater In Shallow/Deep Bore Wells And Relationship With Geological Formations

机译:地下水在浅/深孔井井地球化学和地质构造关系

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Studied area is a tribal area of Warangal District, Andhra Pradesh (A.P.), India. This is (17°42′18″ - 18°36′45″ N and 79°51′04″ - 80°42′23″E) about 4100 sq. km and has different types of rock formation such as granite gneisses, sandstones, pakhals and alluvium etc. This area was facing groundwater problems since two decades. In 1996, National Geophysical Research Institute, Hyderabad did geophysical survey for groundwater exploration collaboration with State Ground Water Department, A.P. Based on geophysical investigation, a large number of drilling sites were recommended and subsequently 40 bore wells were drilled (10.0 to 70.5 m depths). The water table in these bore wells, varies from 5.0 to 15.0 m with discharge rate of 10,000 to 25,000 lit/h. The hydrochemical studies of these waters indicate: 1. Concentrations of aqueous ionic species have changed with different rock types. 2. Groundwaters of granite gneisses areas are more in Total Dissolved Solids (TDS). 3. These groundwaters are classified as Na-Ca-Cl -
机译:学习区是印度州和德拉邦(A.P.)的Warangal区部落区域。这是(17°42'18“ - 18°36'45”N和79°51'04“ - 80°42'23”e)约4100平方公里,并且具有不同类型的岩层,如花岗岩片,砂岩,帕卡尔和肠胃等。这一领域自二十年以来正面临地下水问题。 1996年,国家地球物理研究所,海德拉巴对地下水勘探与国家地下水部门的地球物理调查进行了地层调查,建议大量钻井场所,随后钻出40孔井(深度10.0至70.5米) 。这些钻孔井中的水桌子从5.0到15.0米各不等,排放率为10,000至25,000升/小时。这些水的水化学研究表明:1。含水离子物质的浓度随不同的岩石类型而变化。 2.花岗岩片状地区的地下水更加溶解固体(TDS)。这些地下水被归类为NA-CA-CL -

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